Observations of thermohaline staircases disrupted by mesoscale eddies in the eastern Caribbean Sea from marine seismic data
ID:1360 View Protection:ATTENDEE Updated Time:2024-10-14 15:46:22 Hits:734 Poster Presentation

Start Time:2025-01-16 17:35(Asia/Shanghai)

Duration:15min

Session:S46 Session 46-Oceanic Mesoscale and Submesoscale Processes: Characteristics, Dynamics & Parameterizations » S46-POceanic Mesoscale and Submesoscale Processes: Characteristics, Dynamics & Parameterizations

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Abstract
Thermohaline staircases and mesoscale eddies play crucial roles in the transport of heat, salt, and nutrients in the ocean, yet their complex relationship remains unclear due to the limitations in observational resolution and lateral range. Here, utilizing high spatial resolution seismic images with a total length of 2518 km, we show the widespread occurrence of thermohaline staircases in the eastern Caribbean Sea and demonstrate their three-dimensional distribution. These staircases occupy about 70% of the total length of the seismic lines, with the remaining 30% occupied by six subsurface mesoscale eddies. These staircases are disrupted and interrupted due to the enhanced turbulent diffusivity driven by the vertical shear of these eddies. The numerous high-resolution seismic observations presented herein enhance our comprehension of the interplay between staircases and multiscale oceanic dynamical processes.
 
Keywords
oceanic mesoscale eddy,Thermohaline staircase,seismic oceanography
Speaker
Shun Yang
Undergraduate Tongji University

Submission Author
Shun Yang Tongji University
Kun Zhang Tongji University
Haibin Song Tongji University
Barry Ruddick Dalhousie University
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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